Biogenic and anthropogenic sources of isoprene and monoterpenes and theirsecondary organic aerosol in Delhi, India
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388955%3A_____%2F23%3A00567429" target="_blank" >RIV/61388955:_____/23:00567429 - isvavai.cz</a>
Výsledek na webu
<a href="https://hdl.handle.net/11104/0347419" target="_blank" >https://hdl.handle.net/11104/0347419</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5194/acp-23-61-2023" target="_blank" >10.5194/acp-23-61-2023</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Biogenic and anthropogenic sources of isoprene and monoterpenes and theirsecondary organic aerosol in Delhi, India
Popis výsledku v původním jazyce
Isoprene and monoterpene emissions to the atmosphere are generally dominated by biogenic sources. The oxidation of these compounds can lead to the production of secondary organic aerosol, however the impact of this chemistry in polluted urban settings has been poorly studied. Isoprene and monoterpenes can form secondary organic aerosol (SOA) heterogeneously via anthropogenic-biogenic interactions, resulting in the formation of organosulfate (OS) and nitrooxy-organosulfate (NOS) species. Delhi, India, is one of the most polluted cities in the world, but little is known about the emissions of biogenic volatile organic compounds (VOCs) or the sources of SOA. As part of the DELHI-FLUX project, gas-phase mixing ratios of isoprene and speciated monoterpenes were measured during pre- and post-monsoon measurement campaigns in central Delhi. Nocturnal mixing ratios of the VOCs were substantially higher during the post-monsoon (isoprene: (0.65 +/- 0.43) ppbv, limonene: (0.59 +/- 0.11) ppbv, alpha-pinene: (0.13 +/- 0.12) ppbv) than the pre-monsoon (isoprene: (0.13 +/- 0.18) ppbv, limonene: 0.011 +/- 0.025 (ppbv), alpha-pinene: 0.033 +/- 0.009) period. At night, isoprene and monoterpene concentrations correlated strongly with CO during the post-monsoon period. Filter samples of particulate matter less than 2.5 mu m in diameter (PM2.5) were collected and the OS and NOS content analysed using ultra-high-performance liquid chromatography tandem mass spectrometry (UHPLC-MS2). Inorganic sulfate was shown to facilitate the formation of isoprene OS species across both campaigns. Sulfate contained within OS and NOS species was shown to contribute significantly to the sulfate signal measured via AMS. Strong nocturnal enhancements of NOS species were observed across both campaigns. The total concentration of OS and NOS species contributed an average of (2.0 +/- 0.9) % and (1.8 +/- 1.4) % to the total oxidized organic aerosol and up to a maximum of 4.2 % and 6.6 % across the pre- and post-monsoon periods, respectively. Overall, this study provides the first molecular-level measurements of SOA derived from isoprene and monoterpene in Delhi and demonstrates that both biogenic and anthropogenic sources of these compounds can be important in urban areas.
Název v anglickém jazyce
Biogenic and anthropogenic sources of isoprene and monoterpenes and theirsecondary organic aerosol in Delhi, India
Popis výsledku anglicky
Isoprene and monoterpene emissions to the atmosphere are generally dominated by biogenic sources. The oxidation of these compounds can lead to the production of secondary organic aerosol, however the impact of this chemistry in polluted urban settings has been poorly studied. Isoprene and monoterpenes can form secondary organic aerosol (SOA) heterogeneously via anthropogenic-biogenic interactions, resulting in the formation of organosulfate (OS) and nitrooxy-organosulfate (NOS) species. Delhi, India, is one of the most polluted cities in the world, but little is known about the emissions of biogenic volatile organic compounds (VOCs) or the sources of SOA. As part of the DELHI-FLUX project, gas-phase mixing ratios of isoprene and speciated monoterpenes were measured during pre- and post-monsoon measurement campaigns in central Delhi. Nocturnal mixing ratios of the VOCs were substantially higher during the post-monsoon (isoprene: (0.65 +/- 0.43) ppbv, limonene: (0.59 +/- 0.11) ppbv, alpha-pinene: (0.13 +/- 0.12) ppbv) than the pre-monsoon (isoprene: (0.13 +/- 0.18) ppbv, limonene: 0.011 +/- 0.025 (ppbv), alpha-pinene: 0.033 +/- 0.009) period. At night, isoprene and monoterpene concentrations correlated strongly with CO during the post-monsoon period. Filter samples of particulate matter less than 2.5 mu m in diameter (PM2.5) were collected and the OS and NOS content analysed using ultra-high-performance liquid chromatography tandem mass spectrometry (UHPLC-MS2). Inorganic sulfate was shown to facilitate the formation of isoprene OS species across both campaigns. Sulfate contained within OS and NOS species was shown to contribute significantly to the sulfate signal measured via AMS. Strong nocturnal enhancements of NOS species were observed across both campaigns. The total concentration of OS and NOS species contributed an average of (2.0 +/- 0.9) % and (1.8 +/- 1.4) % to the total oxidized organic aerosol and up to a maximum of 4.2 % and 6.6 % across the pre- and post-monsoon periods, respectively. Overall, this study provides the first molecular-level measurements of SOA derived from isoprene and monoterpene in Delhi and demonstrates that both biogenic and anthropogenic sources of these compounds can be important in urban areas.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10403 - Physical chemistry
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2023
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Atmospheric Chemistry and Physics
ISSN
1680-7316
e-ISSN
1680-7324
Svazek periodika
23
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
23
Strana od-do
61-83
Kód UT WoS článku
000906754100001
EID výsledku v databázi Scopus
2-s2.0-85147288646